We present the first observational evidence for a circumplanetary disk around the protoplanet PDS~70~b, based on a new spectrum in the band acquired with VLT/SINFONI. We tested three hypotheses to explain the spectrum: Atmospheric emission from the planet with either (1) a single value of extinction or (2) variable extinction, and (3) a combined atmospheric and circumplanetary disk model. Goodness-of-fit indicators favour the third option, suggesting circumplanetary material contributing excess thermal emission — most prominent at m. Inferred accretion rates ($\sim 10^{-7.8}10^{-7.3} M_J^{-1}$) are compatible with observational constraints based on the H and Br lines. For the planet, we derive an effective temperature of 1500–1600 K, surface gravity $\log(g)\sim 4.0\sim 1.6 R_J\sim 10 M_J$, and possible thick clouds. Models with variable extinction lead to slightly worse fits. However, the amplitude (mag) and timescale of variation (~years) required for the extinction would also suggest circumplanetary material.

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